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Clues to Earth’s Past

Clues to Earth’s Past

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Clues to Earth’s Past. Fossils. Remains, imprints, or traces of prehistoric organism. Permineralized remains. Fossils where the spaces inside are filled with minerals. Carbon Film. A flim of carbon can form around an organism creating a silhouette. Mold-Cast. - PowerPoint PPT Presentation

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Page 1: Clues to Earth’s Past

Clues to Earth’s Past

Page 2: Clues to Earth’s Past

Remains, imprints, or traces of prehistoric organism.

Fossils

Page 3: Clues to Earth’s Past

Fossils where the spaces inside are filled with minerals

Permineralized remains

Page 4: Clues to Earth’s Past

A flim of carbon can form around an organism creating a silhouette

Carbon Film

Page 5: Clues to Earth’s Past

Mold- imprint left after hard parts of organism decay

Cast- a copy of organism made from the mold

Mold-Cast

Page 6: Clues to Earth’s Past

Fossils that are evidence of organisms activity (not organism itself)

Such as:Tracks/footprintsBurrowsTrails

Trace Fossils

Page 7: Clues to Earth’s Past

Abundant, widespread organisms that existed for a SHORT period of time.

Index Fossils

Page 8: Clues to Earth’s Past

In undisturbed layers of rock, the oldest rocks are found at the bottom, with the rocks becoming younger towards the top.

Principle of Superposition

Page 9: Clues to Earth’s Past

Relative age is how old a rock or fossil is in COMPARISON to the ages of other things.

Relative Age

Page 10: Clues to Earth’s Past

when an igneous intrusion cuts across a formation of rock, it can be determined that the igneous intrusion is younger than the rock it’s cutting through.

Igneous Intrusion

Page 11: Clues to Earth’s Past

Unconformities are when layers of rock are missing

Unconformities develop when running water or glaciers remove rock layers

Unconformities

Page 12: Clues to Earth’s Past

When rock layers are tilted and younger sediment layers are deposited horizontally on top of the eroded and tilted layers

Angular

Page 13: Clues to Earth’s Past

When a layer of horizontal rock is exposed and eroded before younger rocks form over it

Disconformity

Page 14: Clues to Earth’s Past

When sedimentary rock forms over eroded metamorphic or igneous rock

Nonconformity

Page 15: Clues to Earth’s Past

The same rock layers can be found in different locations; FOSSILS must be used to prove that the layers match up

When the layers are too disturbed:

Page 16: Clues to Earth’s Past

Calculating the absolute age of a rock by measuring the amounts of materials in a rock and knowing the material’s half life.

Absolute Dating

Page 17: Clues to Earth’s Past

Half-Life: Time it takes for half of the atoms

in an isotope to decay

Page 18: Clues to Earth’s Past

Breaking down of an atom into a proton and an electron.

Radioactive Decay

Page 19: Clues to Earth’s Past

Uses the properties of atoms in rocks and other object to determine their ages.

Radiometric Dating

Page 20: Clues to Earth’s Past

Principle that Earth’s processes occurring today are similar to those that occurred in the past.

Uniformitarianism